Krakatau

It is said that Krakatoa caused the most serious volcanic eruption in history in 1883. Ancient Krakatoa was formed in 416 AD and still exists in Indonesia. The same explosion that caused a 130-foot tsunami in 1883 destroyed 130 coastal houses, two terminals (India and Australia) and issued approximately 36,000 deaths. It makes a very loud sound, far from Madagascar, about 3,000 miles from the island of Krakata. Some people even think that this may be reasons for temperature drop and spectacular sunset over the next three years.

Krakatoa came out several times in its "lifetime", but this article shared only about three eruptions: 1883, 1988 and 1992. In 1883, Krakatoa made the most dangerous explosion on August 27. Literally, it blew! 75% were destroyed with many other people living near coastline in Australia and India. In 1988, Krakatoa broke up in February, then followed on March 16th. It is reported that the new crater caused two small lava flows that lasted until April, causing a frequent explosion that spurs a small fire. The last eruption we discuss is in 1992. On November 12, the most intense activity of the explosion occurred when Krakatoa began "shooting" a lava bomb from the crater on the northern coast.

We know volcanic eruption, but how did they happen? As a result of several studies, I discovered that they were caused by gas pressure molten magma and forced magma to push up weak areas of the crust. Therefore, this allows magma to be extruded through the volcanic holes, be ejected from the crater, and become lava. On the volcanic eruption of 1883, the volcanic eruption lasted from August 23 to 27. In 1988, the explosion lasted from February to April and continued to explode. In 1992, it continued from November 7, 1992 to August 14, 1993, and it was one of the longest volcanic eruption in Krakatoa. In 1992 the lava flowed 1 kilometer north and moved the coast 100 meters more than the original coast.

Krakatau is still active. During the famous volcanic eruption of 1883, the vibrant ventilation was located in the middle of the crater of the volcano filled with the sea. The island is known as Anak Krakatau, which means Krakatau children. It almost always erupted at a low level, but one or two volcanic eruptions in a year are slightly bigger and some people noticed and reported from time to time. Of course, these are not the size of the famous eruption of 1883. The possibility of explosive occurrence in 1883 is temporarily very small. But going to Anakh Krakataau is undoubtedly dangerous, especially if it is more exciting feelings. It might not be that prudent to spend too much time on a small island that formed the ruins of the main island of Krakato. This is because even a small collapse of Anak Krakatau may create a small tsunami that may have been swept through these islands.

Krakatoa, or Krakatau (Indonesian: Krakatau) is a volcanic island located in Su-Strait between Java Island of Indonesia and Namibia. This name was also used for groups of surrounding islands. This included the remnants of the larger three volcanic peaks that were destroyed in the catastrophic outbreak of 1883. The estimated volcanic eruption index (VEI) is 6 and the eruption is equivalent to 200 megatons of TNT (840 PJ) - destroying Japan's Hiroshima, about 13,000 times the nuclear production of small bombs (13 to 16 knots), Zalbamba 10,000 tons) is four times as large as the most powerful nuclear device that has exploded so far.